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Sökning: onr:"swepub:oai:lup.lub.lu.se:d927ff27-a228-406c-a70b-a09387c4f145" > Separating Si phase...

Separating Si phases from diagenetically-modified sediments through sequential leaching.

Huang, Tzu-Hao (författare)
Stockholms universitet,Stockholm University,Institutionen för geologiska vetenskaper
Sun, Xiaole, 1983- (författare)
Stockholms universitet,Stockholm University,Institute of Oceanology, Chinese Academy of Sciences,Stockholms universitets Östersjöcentrum,Chinese Academy of Sciences, China
Somelar, Peeter (författare)
University of Tartu
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Kirsimae, Kalle (författare)
University of Tartu
Pickering, Rebecca (författare)
Lund University,Lunds universitet,Berggrundsgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Lithosphere and Biosphere Science,Department of Geology,Faculty of Science
Kim, Ji-Hoon (författare)
Korea Institute of Geoscience and Mineral Resources
Kielman-Schmitt, Melanie (författare)
Swedish Museum of Natural History
Hong, Wei-Li, 1982- (författare)
Stockholms universitet,Stockholm University,Institutionen för geologiska vetenskaper,Stockholms universitets Östersjöcentrum
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 (creator_code:org_t)
2023
2023
Engelska.
Ingår i: Chemical Geology. - 0009-2541 .- 1872-6836.
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • Silicon (Si) phases such as biogenic silica, lithogenic silicate and authigenic silica/silicate in marine sediments provide valuable information about past Si cycling. Wet-chemical sequential leaching methods are often applied to extract different Si phases from marine sediments to study Si diagenetic processes in shallow subsurface. The potential of this method to separate Si phases from deeply-buried and diagenetically-modified sediments has not been systematically examined. We applied a sequential leaching protocol to drill core sediments retrieved from the Ulleung Basin, East/Japan Sea. We performed geochemical (elemental abundance and stable Si isotopes, δ30Si) and microscopic (X-ray diffraction and scanning electron microscope) analyses to monitor leaching efficiency in separating different Si phases. We show that, prior to alkaline leaching, applying weak acid is able to remove metal oxide and/or clay-like phases. The following Na2CO3 leaching, based on a commonly-adopted protocol, is able to dissolve some but not all diatoms. The results of elemental contents and δ30Si values of leachates suggest that, in diagenetically-modified sediments, either a longer digesting time or a harsher alkaline leaching is needed to dissolve all diatoms. This is attributed to increased resistance of diatoms to Na2CO3 leaching as a result of reduced surface area and/or improved SiO2 tetrahedron ordering during diagenetic processes over time and burial depths. Lithogenic silicate minerals can be dissolved by NaOH and potentially separated from diatoms if the latter is completely removed in the preceding leaching steps. Even if a trace amount of diatom is left undissolved in the NaOH leaching, it is still possible to separate the two through a mass balance calculation given the knowledge of composition for the two end-members. We conclude that a successful separation of Si phases in diagenetically modified sediments relies on the knowledge of elemental abundance and even δ30Si values of the leachates, as well as information such as species of Si-skeleton organisms, contents and maturation degree of biogenic silica.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geokemi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geochemistry (hsv//eng)

Nyckelord

Silicon
Sequential Leaching
Sediment Phase

Publikations- och innehållstyp

art (ämneskategori)
ref (ämneskategori)

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